By. Lorelei Ing
 The first sedimentary rocks were formed
more than 3.8 billion years ago
 Earth was form 4.6 billion years ago
 The earliest living creatures were
microscopic bacteria
 During this time
period the animals
are more evolved
and more diverse
with features such
as hard shells and
they were able to
hunt, burrow and
crawl
 Trilobite fossil
 Some of the earliest
creatures
 This period lasted
nearly 43 million years
and known for there
diverse marine
invertebrates which
were mainly trilobites
 Earth’s sea levels
raised due to the
melting of glaciers
 Scientist have also
discovered that this
showed the first clear
evidence of life on land
and giant sea
scorpions
 This was a important
stage in the evolution on
life because the first
vertebrates were
starting to come out of
the water and we had
the first wingless bugs.
 The two supercontinents
Gondwana and
Euramerica collided then
made one
supercontinent know as
Pangea.
Carboniferous had
many swaps that then
over time created coal
 A great portion of the marine invertebrates
animals had been extinct
 At that time the only continent that was
separate from the others is what is know Asia
 This is the time when the supercontinent
known as Pangea was altering its ocean
circulation and global climate
dinosaurs are walking on the land
and they mainly eat the ferns
 The oceans are filled with squid
and ammonites
 There are the first birds too exist
 This is the time period when there was the first
fossils of the more recent mammals, certain
groups of birds and some flowering plants.
a fossil
of a bird
 The dinosaurs and marine mammals had
been died completely out and instead
rodents appeared
 Mountains began to arise
 Since it was so cold certain species died out
 Animals like elephant and apes traveled from
Africa to Eurasia
 The supercontinent Pangea had began to
break up
 The mammals were beginning to have fur
coat.
 Info on Cambrian
http://www.bbc.co.uk/nature/history_of_the_earth/Cambria
n
 Info on Ordovician
http://www.ucmp.berkeley.edu/ordovician/ordovician.php
 Info on Silurian
http://www.ucmp.berkeley.edu/silurian/silurian.php
 Info on Devonian
http://www.ucmp.berkeley.edu/devonian/devonian.php
 Info on Carboniferous
http://www.ucmp.berkeley.edu/carboniferous/carboniferous
.php
 Info on the Permian
http://www.ucmp.berkeley.edu/permian/permian.php
 Precambrian from
http://science.nationalgeographic.com/science/prehistoric-
world/precambrian/
Triassic from
http://www.ucmp.berkeley.edu/mesozoic/triassic/triassic.html
Jurassic from
http://www.ucmp.berkeley.edu/mesozoic/jurassic/jurassic.php
Cretaceous from
http://www.ucmp.berkeley.edu/mesozoic/cretaceous/cretaceous.php
Paleogene from
http://science.nationalgeographic.com/science/prehistoric-world/paleogene/
Neogene from
http://science.nationalgeographic.com/science/prehistoric-
world/neogene/#close-modal
Quaternary from
http://science.nationalgeographic.com/science/prehistoric-world/quaternary/

Eras of the earth

  • 1.
  • 2.
     The firstsedimentary rocks were formed more than 3.8 billion years ago  Earth was form 4.6 billion years ago  The earliest living creatures were microscopic bacteria
  • 3.
     During thistime period the animals are more evolved and more diverse with features such as hard shells and they were able to hunt, burrow and crawl  Trilobite fossil  Some of the earliest creatures
  • 4.
     This periodlasted nearly 43 million years and known for there diverse marine invertebrates which were mainly trilobites
  • 5.
     Earth’s sealevels raised due to the melting of glaciers  Scientist have also discovered that this showed the first clear evidence of life on land and giant sea scorpions
  • 6.
     This wasa important stage in the evolution on life because the first vertebrates were starting to come out of the water and we had the first wingless bugs.  The two supercontinents Gondwana and Euramerica collided then made one supercontinent know as Pangea.
  • 7.
    Carboniferous had many swapsthat then over time created coal
  • 8.
     A greatportion of the marine invertebrates animals had been extinct  At that time the only continent that was separate from the others is what is know Asia
  • 9.
     This isthe time when the supercontinent known as Pangea was altering its ocean circulation and global climate
  • 10.
    dinosaurs are walkingon the land and they mainly eat the ferns  The oceans are filled with squid and ammonites  There are the first birds too exist
  • 11.
     This isthe time period when there was the first fossils of the more recent mammals, certain groups of birds and some flowering plants. a fossil of a bird
  • 12.
     The dinosaursand marine mammals had been died completely out and instead rodents appeared
  • 13.
     Mountains beganto arise  Since it was so cold certain species died out  Animals like elephant and apes traveled from Africa to Eurasia
  • 14.
     The supercontinentPangea had began to break up  The mammals were beginning to have fur coat.
  • 15.
     Info onCambrian http://www.bbc.co.uk/nature/history_of_the_earth/Cambria n  Info on Ordovician http://www.ucmp.berkeley.edu/ordovician/ordovician.php  Info on Silurian http://www.ucmp.berkeley.edu/silurian/silurian.php  Info on Devonian http://www.ucmp.berkeley.edu/devonian/devonian.php  Info on Carboniferous http://www.ucmp.berkeley.edu/carboniferous/carboniferous .php  Info on the Permian http://www.ucmp.berkeley.edu/permian/permian.php
  • 16.
     Precambrian from http://science.nationalgeographic.com/science/prehistoric- world/precambrian/ Triassicfrom http://www.ucmp.berkeley.edu/mesozoic/triassic/triassic.html Jurassic from http://www.ucmp.berkeley.edu/mesozoic/jurassic/jurassic.php Cretaceous from http://www.ucmp.berkeley.edu/mesozoic/cretaceous/cretaceous.php Paleogene from http://science.nationalgeographic.com/science/prehistoric-world/paleogene/ Neogene from http://science.nationalgeographic.com/science/prehistoric- world/neogene/#close-modal Quaternary from http://science.nationalgeographic.com/science/prehistoric-world/quaternary/